Results 211 to 220 of about 60,105 (298)
Stability of the marine nitrogen cycle over the past 165 million years. [PDF]
Godfrey LV +5 more
europepmc +1 more source
Acidification Stimulates N2O Production by Oceanic Nitrifying Bacteria
Abstract Recent studies have shown changes in the production rates of nitrous oxide (N2O) in aerobic seawater in response to ocean acidification (OA). Understanding how N2O production responds to OA is crucial because N2O is a strong greenhouse gas and stratospheric ozone‐depleting substance emitted from the ocean.
Sakae Toyoda +5 more
wiley +1 more source
Unexpected microbial rhodopsin dynamics in sync with phytoplankton blooms. [PDF]
Gómez-Consarnau L +9 more
europepmc +1 more source
Abstract The concentration of chlorophyll‐α $\alpha $ has been estimated from sea color, primarily based on the reflectance ratio between the blue and green spectral bands in multiband images obtained by satellite optical sensors. However, this method is only effective in open, clear water and cannot be reliably applied to shallow coastal waters.
Satoru Yamamoto +5 more
wiley +1 more source
Crustal constraints on the surface expression of mantle upwelling in a back-arc passive margin setting. [PDF]
Hwang JY, Chang SJ, Sohn YJ, Kim KH.
europepmc +1 more source
Tracing Coupled GCM Equatorial Pacific Climatological Biases via Surface Flux Adjustments
Abstract Global weather and climate forecasts hinge on the ability of coupled general circulation models (CGCMs) to simulate ocean‐atmosphere interactions in the tropical Pacific. Yet most CGCMs develop tropical Pacific biases, such as an overly‐intense equatorial cold tongue (ECT), which limit their simulation skill.
Xian Wu +4 more
wiley +1 more source
Spatio-temporal patterns, trends, and oceanographic drivers of whale shark strandings in Indonesia. [PDF]
Putra MIH +15 more
europepmc +1 more source
Rethinking Seawater Mo Isotope Mass‐Balance and the Sedimentary Mo Record
Abstract A lingering misconception is that seawater 98Mo/95Mo ratios should have increased more or less linearly with the oxygenation of Earth's oceans. At the root of this hypothesis is the generalization that oxidizing marine sediments have a stronger affinity for lighter‐mass Mo isotopes than their reducing counterparts.
C. M. Ostrander, O. Dellwig
wiley +1 more source

